aenigmatite

{{infobox mineral | name = Aenigmatite | image = Aenigmatite - Mineralogisches Museum Bonn2.jpg | imagesize = 260px | alt = | caption = Aenigmatite from Kangerdluarsuk, Greenland | category = Inosilicates | formula = Na2Fe2+5TiSi6O20 |IMAsymbol=Aen | molweight = | strunz = 9.DH.40 | dana = | system = Triclinic | class = Pinacoidal () (same H-M symbol) | symmetry = P | unit cell = a = 10.415(1), b = 10.840(1) c = 8.931(1) [Å]; Z = 2 α = 105.107(4)° β = 96.610(5)° γ = 125.398(4)° | color = Velvet-black | colour = | habit = Poorly developed prismatic crystals, occurring as irregular clusters; pseudomonoclinic | twinning = Complex by rotation perpendicular to (01) or about [010] of the pseudomonoclinic cell; polysynthetic | cleavage = Good on {010} and {100} | fracture = Uneven | tenacity = Brittle | mohs = 5.5 | luster = Vitreous to greasy | streak = Reddish brown | diaphaneity = Translucent to opaque | gravity = 3.81 | density = | polish = | opticalprop = Biaxial (+) | refractive = nα = 1.780 – 1.800 nβ = 1.800 – 1.820 nγ = 1.870 – 1.900 | birefringence = δ = 0.090 – 0.100 | pleochroism = X = yellow brown; Y = red-brown; Z = dark brown to black | 2V = Measured: 27° to 55° | dispersion = r 2Fe2+5TiSi6O20 and its structure consists of single tetrahedral chains with a repeat unit of four and complex side branches. It forms brown to black triclinic lamellar crystals. It has Mohs hardness of 5.5 to 6 and specific gravity of 3.74 to 3.85. Aenigmatite forms a solid-solution series with wilkinsonite, Na2Fe2+4Fe3+2Si6O20.

Aenigmatite is primarily found in peralkaline volcanic rocks, pegmatites, and granites as well as silica-poor intrusive rocks. It was first described by August Breithaupt in 1865 for an occurrence in the Ilimaussaq intrusive complex of southwest Greenland. Its name comes from αίνιγμα, the Greek word for "riddle".